Stratigraphy Statfjord Fm

Slides:



Advertisements
Similar presentations
Astronaut photo of Delta
Advertisements

Norwegian Interactive Offshore Stratigraphic Lexicon
GE Sedimentary processes and products
Stratigraphy Statfjord Fm
Deltaic Depositional Systems
The Petroleum System- From Source to Trap
Structures and other features within sedimentary rocks - clues to the past environments Paleoenvironments Environment of deposition Direction of water.
HYDROCARBON PETROLEUM SYSTEM
S EDIMENTOLOGY AND SEQUENCE STRATIGRAPHY OF THE M IDDLE -U PPER J URASSIC K ROSSFJORD AND F ENSFJORD FORMATIONS, T ROLL F IELD, NORTHERN N ORTH S EA Richard.
Marginal Marine and Open-Shelf Environments
 The specification says:  Describe the deposition in deltaic environments of delta top (topsets) to form coal, sandstones of the delta slope (foresets)
Coasts Form of sediment is highly dependent on the effect of tides, wave activity and degree of clastic input from rivers. Microtidal coasts: Usually stormed.
Marginal Marine Environments
Marginal-Marine Environments
Estuaries: Background and Definitions Professor Mike Elliott, Institute of Estuarine & Coastal Studies, University of Hull, University of Hull, HU6 7RX,
Professor Chris Kendall
Geological Modeling: Deterministic and Stochastic Models
EARLY PALEOZOIC EVENTS ORDOVICIAN PALEOGEOGRAPHY Cratonic Sequences of
Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,
Features of depositional environments
SEDIMENTARY ARCHIVES Marine Environment SEDIMENTARY ARCHIVES Marine Environment Continental Shelf Flat, smooth regions that fringe continents Few km.
Figure 1.1 The observer in the truck sees the ball move in a vertical path when thrown upward. (b) The Earth observer views the path of the ball as a parabola.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 3 Earth’s Materials Reference: Chapters 2, 3, 6,
Rune Instefjord Project leader, Gullfaks IOR
Professor Chris Kendall
Statfjord - General Information Geography
Continental Shelves. Morphology of continental shelf.
Estuaries An estuary is where a river meets the sea or ocean.
MESOZOIC STRATIGRAPHY BIG HORN AND POWER RIVER BASINS.
Bureau of Economic Geology, The University of Texas
COASTAL DEPOSITIONAL FEATURES
Sedimentary Geology Geos 240 – Chapter 10 Sequence Stratigraphy Dr. Tark Hamilton Dr. Tark Hamilton Readings from Sediments & Basins: (10:1-22) Readings.
Maximising reservoir information from conventional cores – case study 1 Andrew Thurlow Principal Reservoir Geologist Ichron United Kingdom 6 th June 2014.
Fig. 3.4 Lower Brent Stratigraphy. Fig. 3.5 Lower Brent Stratigraphy.
Barrier Islands ….
Classification: Statoil Internal Status: Draft Rezonation of the Åre Formation Heidrun Field, Norwegian Sea Arve Næss (1), Camilla Thrana (1), Mali Brekken.
The Tools of Subsurface Analysis
A Brief Introduction to Sequence Stratigraphy. The Sea Level Record.
Estuary Environments Salmon River/Cobequid Estuary, Nova Scotia.
Biology and Geology 3. Secondary Education COASTAL FEATURES Surface process UNIT 8.
Session 4: Barrier Island, Dunes, Salt Marshes. Room Assignments Students that have all payments completed and all forms returned will be able to sign.
Some Types of Coastlines A closer look at: Estuaries, Deltas and Barrier Islands.
The Chesapeake Bay Estuary
Refresher Lecture 1A Sedimentary Rocks, Facies, and Stacking Patterns
Delta Environments Nile Delta Mississippi Delta.
Our Beaches Are Funky Strange shapes.
Jorge O. Codignotto Buenos Aires University, Argentina
by Aitor A. Ichaso, and Robert W. Dalrymple
(Based on Subsurface Studies) Ashkan Vafadar1, Massih Afghah2
Systems Tracts and Sequence Stratigraphic Surfaces
Estuary Landforms and Features
Seafloor Features Unit 3.
Strand Plain Geometry, Stratigraphy, and Evolution:
6th Grade Earth Science October 2017
North Carolina’s Outer Banks
Seafloor Features Unit 3.
하구및 연안생태Coastal management
Wave refraction and waves breaking into surf
Transgressions and regressions: the key to Earth history
Stratigraphic Traps – Sub-Unconformity & Reef
Introduction to the Gulltopp Satellite Field
FORCE Statfjord & Triassic Formations Workshop at NPD
Shoreline Features Ch
하구및 연안생태Coastal management
6th Grade Earth Science October 2017
by D. J. Went, R. V. Hamilton, N. H. Platt, and J. R. Underhill
River Erosion Erosion shapes the land in different ways as the river moves from its source to its mouth: Near the source of a river, in the upper course,
Inferred Lithology - Prediction
Journal of the Geological Society
Presentation transcript:

Stratigraphy Statfjord Fm Fig. 2.1 S N B-38 B-13 B-8 A-38 A-33 Raude 1 Raude 2 Raude 3 Raude 4 Raude 5 Eiriksson 1 Nansen Eiriksson 2 A-18 A-13 Amundsen Formation C-33 C-21 C-1A 10m Sand Shale Lunde Formation 1km

Progradation Transgression Retrogradation Fig. 2.2 SOUTH NORTH Nansen Eiriksson 2 Progradation Eiriksson 1 Raude 5 Raude 4 Raude 3 Raude 2 Raude 1

Fluvial Channels 3D model, Raude Fig. 2.3 sand sand shale shale Raude 1 Raude 5

Paleogeography, Cook Fm. Fig. 2.4 Statfjord Field Statfjord Field

Fig. 2.5 Statfjord Field

Fig. 2.6 Brent Paleogeography Broom Rannoch

Fig. 2.7 Brent Paleogeography Etive (lower part) Etive (upper part)

Fig. 2.8 Brent Paleogeography Ness (lower part) Ness (middle part)

Fig. 2.9 Brent Paleogeography Ness (upper part) Tarbert

Fig. 2.10

sand-shale subdivisions Fig. 2.11 Reservoir Zonation Ness Formation sand-shale subdivisions

Ness Sands Fig. 2.12

Fig. 2.13 E1 Sand K2, J2 bay J1 delta (front), bay, fluvial I1 bay, shallow marine H2 bay Tidal & Shallow Marin e H1 fluvial G3, G2 lagoon, bay, shallow marine, tidal G1 bay, tidal bar, lagoon, fluvial, shallow marine E2 lagoon Lagoon E1 fluvial, lagoon, shallow marine, tidal D1 fluvial, shallow marine, lagoon, tidal C2 lagoon, fluvial, shallow marine C1 lagoon, shallow marine, tidal B2 lagoon, shallow marine Fluvial A3 lagoon E1 Sand A2 lagoon, fluvial

Ness (middle part) = C1 -> E2 tid LAGOON RIVERS ETIVE WASHOVERS / BARS SHORELINE SANDS Ness (middle part) = C1 -> E2 tid E1 Sand Fluvial Tidal & Shallow Marin e Lagoon Fig. 2.14

Depositional Environments Ness / Etive Fig. 2.15